La Formación Milanos en el Subbético Medio (Jurásico superior): definición y descripción

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dc.contributor.authorMolina, José Miguel
dc.contributor.authorVera, J. A.
dc.date.accessioned2015-11-23T11:44:53Z
dc.date.available2015-11-23T11:44:53Z
dc.date.issued1996
dc.description.abstractThe Milanos Fm (Upper Kimmeridgian-Tithonian) is defined and characterised as a new formation belonging to the Middle Subbetic (External Zones of the Betic Cordillera). It is composed by marly limestones, marls and calciclastites with chert, but over all it is mainly distinguished by the presence of calcarenitic and calcisiltitic levels with hummocky cross-stratification (HCS). The caltidastic levels are interpreted as storm layers deposited in an outer marine platform or ramp below the fair-weather storm wave base level, in which only the waves generated by the stronger storms would affect the bottomen_US
dc.identifier.urihttp://hdl.handle.net/10272/11403
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accessen_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherMilanos Fmen_US
dc.subject.otherUpper Jurassicen_US
dc.subject.otherMiddle Subbeticen_US
dc.subject.otherTempestitesen_US
dc.titleLa Formación Milanos en el Subbético Medio (Jurásico superior): definición y descripciónen_US
dc.titleThe Milanos Fm in the Middle Subbetic (Upper Jurassic): definition and descriptioneng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 20-1, (1996)